A Fauna-List of the Decapod Crustacea from the Coasts Washed by the Tsushima Warm Current
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A Classification of Living and Fossil Genera of Decapod Crustaceans
RAFFLES BULLETIN OF ZOOLOGY 2009 Supplement No. 21: 1–109 Date of Publication: 15 Sep.2009 © National University of Singapore A CLASSIFICATION OF LIVING AND FOSSIL GENERA OF DECAPOD CRUSTACEANS Sammy De Grave1, N. Dean Pentcheff 2, Shane T. Ahyong3, Tin-Yam Chan4, Keith A. Crandall5, Peter C. Dworschak6, Darryl L. Felder7, Rodney M. Feldmann8, Charles H. J. M. Fransen9, Laura Y. D. Goulding1, Rafael Lemaitre10, Martyn E. Y. Low11, Joel W. Martin2, Peter K. L. Ng11, Carrie E. Schweitzer12, S. H. Tan11, Dale Tshudy13, Regina Wetzer2 1Oxford University Museum of Natural History, Parks Road, Oxford, OX1 3PW, United Kingdom [email protected] [email protected] 2Natural History Museum of Los Angeles County, 900 Exposition Blvd., Los Angeles, CA 90007 United States of America [email protected] [email protected] [email protected] 3Marine Biodiversity and Biosecurity, NIWA, Private Bag 14901, Kilbirnie Wellington, New Zealand [email protected] 4Institute of Marine Biology, National Taiwan Ocean University, Keelung 20224, Taiwan, Republic of China [email protected] 5Department of Biology and Monte L. Bean Life Science Museum, Brigham Young University, Provo, UT 84602 United States of America [email protected] 6Dritte Zoologische Abteilung, Naturhistorisches Museum, Wien, Austria [email protected] 7Department of Biology, University of Louisiana, Lafayette, LA 70504 United States of America [email protected] 8Department of Geology, Kent State University, Kent, OH 44242 United States of America [email protected] 9Nationaal Natuurhistorisch Museum, P. O. Box 9517, 2300 RA Leiden, The Netherlands [email protected] 10Invertebrate Zoology, Smithsonian Institution, National Museum of Natural History, 10th and Constitution Avenue, Washington, DC 20560 United States of America [email protected] 11Department of Biological Sciences, National University of Singapore, Science Drive 4, Singapore 117543 [email protected] [email protected] [email protected] 12Department of Geology, Kent State University Stark Campus, 6000 Frank Ave. -
National Monitoring Program for Biodiversity and Non-Indigenous Species in Egypt
UNITED NATIONS ENVIRONMENT PROGRAM MEDITERRANEAN ACTION PLAN REGIONAL ACTIVITY CENTRE FOR SPECIALLY PROTECTED AREAS National monitoring program for biodiversity and non-indigenous species in Egypt PROF. MOUSTAFA M. FOUDA April 2017 1 Study required and financed by: Regional Activity Centre for Specially Protected Areas Boulevard du Leader Yasser Arafat BP 337 1080 Tunis Cedex – Tunisie Responsible of the study: Mehdi Aissi, EcApMEDII Programme officer In charge of the study: Prof. Moustafa M. Fouda Mr. Mohamed Said Abdelwarith Mr. Mahmoud Fawzy Kamel Ministry of Environment, Egyptian Environmental Affairs Agency (EEAA) With the participation of: Name, qualification and original institution of all the participants in the study (field mission or participation of national institutions) 2 TABLE OF CONTENTS page Acknowledgements 4 Preamble 5 Chapter 1: Introduction 9 Chapter 2: Institutional and regulatory aspects 40 Chapter 3: Scientific Aspects 49 Chapter 4: Development of monitoring program 59 Chapter 5: Existing Monitoring Program in Egypt 91 1. Monitoring program for habitat mapping 103 2. Marine MAMMALS monitoring program 109 3. Marine Turtles Monitoring Program 115 4. Monitoring Program for Seabirds 118 5. Non-Indigenous Species Monitoring Program 123 Chapter 6: Implementation / Operational Plan 131 Selected References 133 Annexes 143 3 AKNOWLEGEMENTS We would like to thank RAC/ SPA and EU for providing financial and technical assistances to prepare this monitoring programme. The preparation of this programme was the result of several contacts and interviews with many stakeholders from Government, research institutions, NGOs and fishermen. The author would like to express thanks to all for their support. In addition; we would like to acknowledge all participants who attended the workshop and represented the following institutions: 1. -
Groundwater Oxygen Isotope Anomaly Before the M6.6 Tottori Earthquake
www.nature.com/scientificreports OPEN Groundwater oxygen isotope anomaly before the M6.6 Tottori earthquake in Southwest Japan Received: 13 December 2017 Satoki Onda1, Yuji Sano 1, Naoto Takahata 1, Takanori Kagoshima1, Toshihiro Miyajima1, Accepted: 8 March 2018 Tomo Shibata2, Daniele L. Pinti 3, Tefang Lan4, Nak Kyu Kim5, Minoru Kusakabe5 & Published: xx xx xxxx Yoshiro Nishio6 Geochemical monitoring of groundwater in seismically-active regions has been carried out since 1970s. Precursors were well documented, but often criticized for anecdotal or fragmentary signals, and for lacking a clear physico-chemical explanation for these anomalies. Here we report – as potential seismic precursor – oxygen isotopic ratio anomalies of +0.24‰ relative to the local background measured in groundwater, a few months before the Tottori earthquake (M 6.6) in Southwest Japan. Samples were deep groundwater located 5 km west of the epicenter, packed in bottles and distributed as drinking water between September 2015 and July 2017, a time frame which covers the pre- and post-event. Small but substantial increase of 0.07‰ was observed soon after the earthquake. Laboratory crushing experiments of aquifer rock aimed to simulating rock deformation under strain and tensile stresses were carried out. Measured helium degassing from the rock and 18O-shift suggest that the co-seismic oxygen anomalies are directly related to volumetric strain changes. The fndings provide a plausible physico- chemical basis to explain geochemical anomalies in water and may be useful in future earthquake prediction research. Hydro-geochemical precursors of major earthquakes have attracted the attention of researchers worldwide, because they are not entirely unexpected1,2. -
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JP9950127 ®n m&?. mti HBA\ /j^¥ m** f «ffe#«i^p^fe«j:y f^± (top-soii) frbzarm (sub-son) '\<Dm$tm*wfeLtz0 i37 ,37 ®mmm(nmij\c£^ffi'Pi-& cs(DfrMim%¥mmmm7^mT\ ££>c cs<z)fe , i3, !^«££1ffiIELfc&JK0*£«fc^«'> tS Cs<Dn<Dffi8¥tmffil*4l~-42Spk%-3tz0 ffi^f.^CTi'N© 137Cs©*»4^iMf^±fc*)1.6~1.7%/^-C&o^o £fc* 1996^K t3, &\fZ Cs<Dft±£*<DTm<D%ttm&*mfeLfcm%\*¥ftX-6:4t1i-it:0 Residence half-time of 137Cs in the top-soils of Japanese paddy and upland fields Misako KOMAMURA, Akito TSUMURA*. Kiyoshi K0DA1RA** National Institute of Agro-Environmental Sciences, *ex-National Institute of Agro-Environmental Sciences, **Prof. Em. Ashikaga Institute of Technology A series of top-soil samples of 14 paddy fields and 10 upland fields in Japan, were annually collected during more than 30 years, to be examined in the contents of ,37Cs. The data, which were obtained by the use of a gamma spectrometric system, received some statistical treatments to distinguish the annual decline of 137Cs contents from deviations. Then the authors calculated "residence half-time of137Cs" within top-soil, and "eluviation rate of 137Cs" from top to the sub-layer of the soil. The following nationwide results were obtained irrespective of paddy or upland fields: (1) The "apparent residence half-time" was estimated as 16—-17 years. This one consists of both effects of eluviation and nuclear disintegration. (2) The "true residence half-time" was reported as 41~~42 years. This one depends on the eluviation speed of 137Cs exclusively, because the influence of nuclear disinte• gration has been compensated. -
China Russia
1 1 1 1 Acheng 3 Lesozavodsk 3 4 4 0 Didao Jixi 5 0 5 Shuangcheng Shangzhi Link? ou ? ? ? ? Hengshan ? 5 SEA OF 5 4 4 Yushu Wuchang OKHOTSK Dehui Mudanjiang Shulan Dalnegorsk Nongan Hailin Jiutai Jishu CHINA Kavalerovo Jilin Jiaohe Changchun RUSSIA Dunhua Uglekamensk HOKKAIDOO Panshi Huadian Tumen Partizansk Sapporo Hunchun Vladivostok Liaoyuan Chaoyang Longjing Yanji Nahodka Meihekou Helong Hunjiang Najin Badaojiang Tong Hua Hyesan Kanggye Aomori Kimchaek AOMORI ? ? 0 AKITA 0 4 DEMOCRATIC PEOPLE'S 4 REPUBLIC OF KOREA Akita Morioka IWATE SEA O F Pyongyang GULF OF KOREA JAPAN Nampo YAMAJGATAA PAN Yamagata MIYAGI Sendai Haeju Niigata Euijeongbu Chuncheon Bucheon Seoul NIIGATA Weonju Incheon Anyang ISIKAWA ChechonREPUBLIC OF HUKUSIMA Suweon KOREA TOTIGI Cheonan Chungju Toyama Cheongju Kanazawa GUNMA IBARAKI TOYAMA PACIFIC OCEAN Nagano Mito Andong Maebashi Daejeon Fukui NAGANO Kunsan Daegu Pohang HUKUI SAITAMA Taegu YAMANASI TOOKYOO YELLOW Ulsan Tottori GIFU Tokyo Matsue Gifu Kofu Chiba SEA TOTTORI Kawasaki KANAGAWA Kwangju Masan KYOOTO Yokohama Pusan SIMANE Nagoya KANAGAWA TIBA ? HYOOGO Kyoto SIGA SIZUOKA ? 5 Suncheon Chinhae 5 3 Otsu AITI 3 OKAYAMA Kobe Nara Shizuoka Yeosu HIROSIMA Okayama Tsu KAGAWA HYOOGO Hiroshima OOSAKA Osaka MIE YAMAGUTI OOSAKA Yamaguchi Takamatsu WAKAYAMA NARA JAPAN Tokushima Wakayama TOKUSIMA Matsuyama National Capital Fukuoka HUKUOKA WAKAYAMA Jeju EHIME Provincial Capital Cheju Oita Kochi SAGA KOOTI City, town EAST CHINA Saga OOITA Major Airport SEA NAGASAKI Kumamoto Roads Nagasaki KUMAMOTO Railroad Lake MIYAZAKI River, lake JAPAN KAGOSIMA Miyazaki International Boundary Provincial Boundary Kagoshima 0 12.5 25 50 75 100 Kilometers Miles 0 10 20 40 60 80 ? ? ? ? 0 5 0 5 3 3 4 4 1 1 1 1 The boundaries and names show n and t he designations us ed on this map do not imply of ficial endors ement or acceptance by the United N at ions. -
Between Arcadia and Crete: Callisto in Callimachus' Hymn to Zeus The
Between Arcadia and Crete: Callisto in Callimachus’ Hymn to Zeus The speaker of Callimachus’ Hymn to Zeus famously asks Zeus himself whether he should celebrate the god as “Dictaean,” i.e. born on Mt. Dicte in Crete, or “Lycaean,” born on Arcadian Mt. Lycaeus (4-7). When the response comes, “Κρῆτες ἀεὶ ψεῦσται” (“Cretans are always liars,” 8), the hymnist agrees, and for support recalls that the Cretans built a tomb for Zeus, who is immortal (8-9). In so dismissing Cretan claims to truth, the hymnist justifies an Arcadian setting for his ensuing birth narrative (10-41). Curiously, however, after recounting Zeus’s birth and bath, the hymnist suddenly locates the remainder of the god’s early life in Crete after all (42-54). The transition is surprising, not only because it runs counter to the previous rejection of Cretan claims, but also because the Arcadians themselves held that Zeus was both born and raised in Arcadia (Paus. 8.38.2). While scholars have focused on how the ambiguity of two place names (κευθμὸν... Κρηταῖον, 34; Θενάς/Θεναί, 42, 43) misleads the audience and/or prepares them for the abrupt move from Arcadia to Crete (Griffiths 1970 32-33; Arnott 1976 13-18; McLennan 1977 66, 74- 75; Tandy 1979 105, 115-118; Hopkinson 1988 126-127), this paper proposes that the final word of the birth narrative, ἄρκτοιο (“bear,” 41), plays an important role in the transition as well. This reference to Callisto a) allusively justifies the departure from Arcadia, by suggesting that the Arcadians are liars not unlike the Cretans; b) prepares for the hymnist’s rejection of the Cretan account of Helice; and c) initiates a series of heavenly ascents that binds the Arcadian and Cretan portions of the hymn and culminates climactically with Zeus’s own accession to the sky. -
Atergatis Roseus Ordine Decapoda (Rüppell, 1830) Famiglia Xanthidae
Identificazione e distribuzione nei mari italiani di specie non indigene Classe Malacostraca Atergatis roseus Ordine Decapoda (Rüppell, 1830) Famiglia Xanthidae SINONIMI RILEVANTI Nessuno. DESCRIZIONE COROLOGIA / AFFINITA’ Tropicale e sub-tropicale settentrionale e Carapace allungato trasversalmente, fortemente meridionale. sub-ovale, convesso, minutamente punteggiato; regioni non definite. Fronte stretta. Antennule ripiegate trasversalmente, setto inter-antennulare DISTRIBUZIONE ATTUALE largo. Margine dorso-orbitale con tre suture, Dal Mar Rosso alle Fiji. peduncoli oculari corti e spessi. Margine antero- laterale molto arcuato, smussato e carenato. Lato PRIMA SEGNALAZIONE IN MEDITERRANEO inferiore del carapace concavo. Chelipedi sub- 1961, Israele (Lewinsohn & Holthuis, 1964). eguali, margine superiore della chela dotato di una cresta smussata. Cresta dorsale anche sul mero degli altri pereiopodi. PRIMA SEGNALAZIONE IN ITALIA - COLORAZIONE Carapace rosso-brunastro scuro, estremità delle dita delle chele nera. Nei giovani, il carapace è ORIGINE arancio-rosso orlato di bianco. Indo-Pacifico FORMULA MERISTICA VIE DI DISPERSIONE PRIMARIE Probabile migrazione lessepsiana attraverso il - Canale di Suez. TAGLIA MASSIMA VIE DI DISPERSIONE SECONDARIE Lunghezza del carapace fino a 60 mm. - STADI LARVALI STATO DELL ’INVASIONE Non nativo - Identificazione e distribuzione nei mari italiani di specie non indigene SPECIE SIMILI MOTIVI DEL SUCCESSO Xanthidae autoctoni Sconosciuti CARATTERI DISTINTIVI SPECIE IN COMPETIZIONE Carapace regolarmente ovale, -
First Mediterranean Record of Actaea Savignii (H. Milne Edwards, 1834) (Crustacea: Decapoda: Brachyura: Xanthidae), an Additional Erythraean Alien Crab
BioInvasions Records (2013) Volume 2, Issue 2: 145–148 Open Access doi: http://dx.doi.org/10.3391/bir.2013.2.2.09 © 2013 The Author(s). Journal compilation © 2013 REABIC Rapid Communication First Mediterranean record of Actaea savignii (H. Milne Edwards, 1834) (Crustacea: Decapoda: Brachyura: Xanthidae), an additional Erythraean alien crab Selahattin Ünsal Karhan1*, Mehmet Baki Yokeş2, Paul F. Clark3 and Bella S. Galil4 1 Division of Hydrobiology, Department of Biology, Faculty of Science, Istanbul University, 34134 Vezneciler, Istanbul, Turkey 2 Department of Molecular Biology & Genetics, Faculty of Arts & Sciences, Haliç University, 34381 Sisli, Istanbul, Turkey 3 Department of Life Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, England 4 National Institute of Oceanography, Israel Oceanographic & Limnological Research, POB 8030, Haifa 31080, Israel E-mail: [email protected] (SÜK), [email protected] (MBY), [email protected] (PFC), [email protected] (BSG) *Corresponding author Received: 19 January 2013 / Accepted: 8 March 2013 / Published online: 16 March 2013 Handling editor: Amy Fowler Abstract To date, the only alien xanthid crab recorded from the Mediterranean is Atergatis roseus (Rüppell, 1830). This species was first collected off Israel in 1961 and is now common along the Levantine coast. Recently a second alien xanthid species, Actaea savignii (H. Milne Edwards, 1834), was found off Israel and Turkey. A single adult specimen was collected in Haifa Bay in 2010, and two specimens were captured off Mersin, Turkey in 2011. Repeatedly reported from the Suez Canal since 1924, the record of the Levantine populations of A. savignii is a testament to the ongoing Erythraean invasion of the Mediterranean Sea. -
Greek Island Odyssey Holiday Report 2013
Greek Island Odyssey Holiday Report 2013 Day 1: Saturday 20th April As our plane came in to land at Rhodes airport the wildlife spotting began! We had a good view of a female Marsh Harrier and Little Egret over the nearby river. Then, on the drive to the hotel, we saw a Wood Sandpiper on the same river by the road bridge. Upon our arrival in the medieval old town Andy and Denise made a quick foray into the moat and town and found Starred Agamas, Oertzen’s Rock Lizards, a Dahl’s Whip Snake and Large Wall Brown butterflies. It was late evening by then and so we sat at a local taverna for our first traditional Greek mezedes meal and discussed plans for the week ahead over a civilized glass of wine. Day 2: Sunday 21st April After a hearty breakfast at the hotel we set off on our first Anatolian Worm Lizard full day of exploration. Our first stop was the archaeological park at Monte Smith. After parking the car and with lots of butterflies flying around us, it was hard to know just what to look at first. Andy diverted our attention, announcing that he had found an Anatolian Worm Lizard, a strange creature looking more like a worm than a lizard and which is found in Turkey and Greece. On Rhodes it is recorded only in the northern parts of the island. Lesser Fiery Copper We then moved on to watch the butterflies. The first two we identified were male and female Lesser Fiery Coppers, soon followed by Eastern Bath White, and Clouded yellow. -
Distribution, Abundance, and Diversity of Epifaunal Benthic Organisms in Alitak and Ugak Bays, Kodiak Island, Alaska
DISTRIBUTION, ABUNDANCE, AND DIVERSITY OF EPIFAUNAL BENTHIC ORGANISMS IN ALITAK AND UGAK BAYS, KODIAK ISLAND, ALASKA by Howard M. Feder and Stephen C. Jewett Institute of Marine Science University of Alaska Fairbanks, Alaska 99701 Final Report Outer Continental Shelf Environmental Assessment Program Research Unit 517 October 1977 279 We thank the following for assistance during this study: the crew of the MV Big Valley; Pete Jackson and James Blackburn of the Alaska Department of Fish and Game, Kodiak, for their assistance in a cooperative benthic trawl study; and University of Alaska Institute of Marine Science personnel Rosemary Hobson for assistance in data processing, Max Hoberg for shipboard assistance, and Nora Foster for taxonomic assistance. This study was funded by the Bureau of Land Management, Department of the Interior, through an interagency agreement with the National Oceanic and Atmospheric Administration, Department of Commerce, as part of the Alaska Outer Continental Shelf Environment Assessment Program (OCSEAP). SUMMARY OF OBJECTIVES, CONCLUSIONS, AND IMPLICATIONS WITH RESPECT TO OCS OIL AND GAS DEVELOPMENT Little is known about the biology of the invertebrate components of the shallow, nearshore benthos of the bays of Kodiak Island, and yet these components may be the ones most significantly affected by the impact of oil derived from offshore petroleum operations. Baseline information on species composition is essential before industrial activities take place in waters adjacent to Kodiak Island. It was the intent of this investigation to collect information on the composition, distribution, and biology of the epifaunal invertebrate components of two bays of Kodiak Island. The specific objectives of this study were: 1) A qualitative inventory of dominant benthic invertebrate epifaunal species within two study sites (Alitak and Ugak bays). -
Family PANDALIDAE the Genera of This Family May
122 L. B. HOLTHUIS Family PANDALIDAE Pandalinae Dana, 1852, Proc. Acad. nat. Sci. Phila. 6: 17, 24. Pandalidae Bate, 1888, Rep. Voy. Challenger, Zool. 24: xii, 480, 625. The genera of this family may be distinguished with the help of the fol- lowing key, which is largely based on the key given by De Man (1920, Siboga Exped. 39 (a3) : 101, 102); use has also been made of Kemp's (1925, Rec. Indian Mus. 27:271, 272) key to the Chlorotocus section of this family. 1. Carpus of second pereiopods consisting of more than three joints. 2 — Carpus of second pereiopods consisting of 2 or 3 joints 13 2. No longitudinal carinae on the carapace except for the postrostral crest. 3 — Carapace with longitudinal carinae on the lateral surfaces. Integument very firm. 12 3. Rostrum movably connected with the carapace Pantomus — Rostrum not movable 4 4. Eyes poorly developed, cornea narrower than the eyestalk . Dorodotes — Eyes well developed, cornea much wider than the eyestalk .... 5 5. Third maxilliped with an exopod 6 — Third maxilliped without exopod 8 6. Epipods on at least the first two pereiopods 7 — No epipods on any of the pereiopods Parapandalus 7. Posterior lobe of scaphognathite broadly rounded or truncate. Stylocerite pointed anteriorly. Rostrum with at least some fixed teeth dorsally. Plesionika — Posterior lobe of scaphognathite acutely produced. Stylocerite broad and rounded. Rostrum with only movable spines dorsally Dichelopandalus 8. Laminar expansion of the inner border of the ischium of the first pair of pereiopods very large Pandalopsis — Laminar expansion of the inner border of the ischium of the first pair of pereiopods wanting or inconspicuous 9 9. -
Justice and Humanity JCG - Keeping the Oceans Safe and Enjoyable for Future Generations! 120°E 130°E 140°E 150°E 160°E 170°E
Justice and Humanity JCG - Keeping the oceans safe and enjoyable for future generations! 120°E 130°E 140°E 150°E 160°E 170°E Territorial sea 165° East Approx. 430,000 km2 (Including inland waters) 5 0 °N Territorial sea + EEZ Approx. 4,470,000 km2 (Japan’s Land area x 12) Etorofu Island Land area Japan Sea 2 Approx. 380,000 km 4 0 °N Takeshima Pacific Ocean Exclusive Economic Zone (EEZ) 2 East China Sea Approx. 4,050,000 km 3 0 °N Senkaku Islands Ogasawara Islands Io To Island Yonagunijima Island Minami-Tori Shima Island 2 0 °N Oki-no-Tori Shima Island 17° North Extended continental shelves* Japan's search responsibility area Approx. 180,000 km2 under the U.S.-Japan SAR Agreement * Areas of the sea as defined in Article 2 (2) of the Exclusive Economic Zone and Continental Shelf Act. For illustration purposes, this map also shows geographical intermediate lines in waters in which borders with neighboring countries have yet to be demarcated. Despite ranking only 61st in the world in terms of land area (380,000 km2), Japan’s territorial waters and exclusive economic zone combined are 12 times larger (4,470,000 km2) than its land area. In December 1986, the Agreement between the Government of the United States of America and the Government of Japan on Maritime Search and Rescue (U.S.-Japan SAR Agreement) was concluded, under which Japan is responsible for coordinating search and rescue activities in the vast expanse of ocean that extends northward from 17° North and westward from 165° East.